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Filtering by: Advisor Hodge, E. T. Non-Academic Affiliation Oregon State University. Graduate School

Rhyolitic epithermal mineralization of the Boulder batholith, Montana

Creator:

Teir, Lennart T.

Resource Type:

Masters Thesis

Full Text:

ACKNOWLEDGEMENTS To Dr. E. T. Hodße who suested the research pose!- bilities present in the area, directed the
Origin of the mineral deposits of north Santiam mining district, Oregon

Creator:

Leever, William Hamilton

Resource Type:

Masters Thesis
A summary of our knowledge of Oregon's igneous geology

Creator:

Harris, Quinton Parker

Resource Type:

Masters Thesis

Full Text:

, No . 1 (2). Hodge, E. T. Progress in Oregon Geology Since 1925. Unive rsity of Oregon Publication
A study of the effects of some medicinal agents on breeding problems of fur-bearing animals

Creator:

Fuhrman, Frederick A.

Resource Type:

Masters Thesis

Full Text:

adn:inis4ration of a cdic- mal t 'ould be necessr:,. uons1derin t .. e difficltcs of c:dL:istr:tion tlis was
An investigation of Oregon grown peppermint

Creator:

Hayden, Alice Hazel, 1909-1994

Resource Type:

Masters Thesis

Full Text:

. T., and Russell, E. R. {1929}. 33 Jll fractions were colorless when first oolleote4
Umbellulone, pharmacological and bactericidal properties

Creator:

Drake, Miles Edward

Resource Type:

Masters Thesis

Full Text:

aad optlcal rotat!.m of,.-28o. srytlr (gg) .t$cc tlut the dry oll her e rolubtllty of 1r10oo la rater
Longitudinal electroproduction of charged pions from Hydrogen, Deuterium, and Helium-3

Creator:

Gaskell, David J.

Abstract:

Conventional pictures of nuclear interactions, in which the pion mediates the long/medium range part of the nuclear force, predict an enhancement of the virtual pion cloud in nuclei relative to that in the free nucleon. Jefferson Lab Experiment E91003 measured charged pion electroproduction from Hydrogen, Deuterium, and Helium-3. The longitudinal...

Resource Type:

Dissertation

Full Text:

transferred to the nucleon(s) and is given by, t = (w E)2 q2 pj2 + 2qpj COSOpq. (1.9) Note that the three